Topic 1: EQ3 Flashcards

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1
Q

Do many tectonic hazards turn into disasters?

A

Very few tectonic hazards manifest themselves into disasters. For example, during the period of 2004-14 tectonic hazards had a low occurrence compared to hydrological and meteorological hazards, and they also have a much lower number of victims compared to the other three hazards (climatological, hydrological, and meteorological).

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2
Q

What are the 4 categories of hazards?

A

-Climatological
-Geophysical
-Hydrological
-Meteorological

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3
Q

What long-term natural hazard trends can be seen since the 1960s?

A

-The total (aggregate) number of recorded hazards has increased.
-The number of reported disasters seems to be falling, having peaked in the early 2000s.
-The number of deaths is lower than in the past, but there are spikes with mega-events.
-The total number of people affected is increasing for some hazard and disaster types, especially meteorological and hydrological
-The economic costs associated with both hazards and disasters has increased significantly.

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4
Q

What are climatological events?

A

Extreme temperatures, droughts and wildfires

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5
Q

What are hydrological events?

A

Floods and mass movement

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6
Q

What are meteorological events?

A

Tropical storms, extra-tropical storms, conventive storms and local storms.

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7
Q

What are geophysical events?

A

Earthquakes, tsunamis and volcanic activity.

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8
Q

How have the different types of hazards increased since 1980?

A

Although tectonic hazards have predominantly remained the same, the other types (especially hydrological and meteorological) appear to be increasing.

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9
Q

How does the trend of geophysical hazards differ from the general trend?

A

In terms of the number of events, it is much more stable, but the number of people affected and number of deaths varies significantly year on year.

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10
Q

Why is the spatial variation of tectonic hazards important?

A

It is wrong to assume that the locations of hazard impacts will always translate into simple distributions. Data shows there is a complex pattern based off of both world regions and levels of development.

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11
Q

Why can disaster statistics be controversial?

A

-Depends on whether both primary and secondary deaths are included.
-Local or regional events in remote places are often under-recorded.
-Can be political bias.
-Stats on major disasters can be extremely difficult to collect
-Time-trend analysis is difficult due to the dependence on intervals selected and whether the methods of collecting the data remain constant. Can be upset by clusters of mega-disasters, e.g the 2011 Haiti Earthquake.

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12
Q

What is an example of disaster statistics being vulnerable to political bias?

A

The 2004 Asian tsunami was almost completely ignored in Myanmar, but also overstated in parts of Thailand, where foreign tourists were killed. This was then played down to protect the Thai tourism industry

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13
Q

What is an example of disaster stats being hard to collect for remote rural areas of low economic development?

A

In the densely populated squatted settlements of the 2003 Caracas landslides.

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14
Q

What are the characteristics of tectonic mega-disasters?

A

-They’re usually large-scale disasters on a aerial or spatial scale, as well as their economic and human impact.
-Their scale poses a serious problem for effective management to minimise both the short and long term impacts, and international aid is often required.
Events will often affect multiple countries (either directly or indirectly).

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15
Q

Why is it an issue that tectonic mega-events are often high-impact, low-probability?

A

This means that there are one-off high profile crises such as the 2010 Haiti earthquake. Due to the low likelihood of occurrence, but the extremely high cost of mitigation actions, regions often are extremely ill-prepared for the event which follows.

For good measure, they’re also extremely difficult to predict.

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16
Q

How do tectonic mega disasters cause economic issues globally?

A

The globalisation of supply chains and production has reduced industry resilience to these events. Hugh-value manufacturing is at risk due to its just-in-time business model. Therefore, a disaster in one location causes major impacts on the other parts of the supply chain in other regions. The Tohoku 2011 earthquake caused a 5% fall in Japan’s GDP, but for TNCs such as Toyota and Sony, production was forced to completely halt.

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17
Q

What was the Eyjafjallajökull, Iceland volcano?

A

In March 2010, the Eyjafjallajökull volcano erupted for the first time in 190 years. It began to affect much of Europe, spreading as far as Northern Italy. It was, however, a relatively small eruption, with no direct deaths, just ‘in the wrong place’.

This grounded flights in most of Europe for days, and 100,000 air journeys were cancelled.

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18
Q

What was the affect of the Eyjafjallajökull volcano on the global supply chain?

A

Due to the shutdown of the air travel, imports and exports into and out of Europe were greatly effected. In the UK, airfreight accounts for 25% of UK trade by value.

High value components in the car manufacturing industry caused firms such as Nissan to halt production, as sensors produced in Ireland couldn’t travel to factories.

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19
Q

What was the impact of the Eyjafjallajökull volcano on the transport of perishable goods?

A

There were impacts on the producers of perishable goods in African countries such as Kenya. The delays in transportation meant that large quantities of fast-perishing produce rotted, leading to losses for producers. The world bank estimated that this will of cost African nations US$65million.

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20
Q

What was the Tohoku tsunami, Japan?

A

A 9.0 magnitude earthquake in March 2011 produced a tsunami which wrecked the east coast of Japan.

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21
Q

What were the regional impacts of the Tohoku tsunami?

A

-15,749 died
-4000 missing
-Large scale Destruction of properties along the coast, as well as damage to infrastructure and the Fukushima nuclear meltdown, causing contaminated water to leak from the plant into the the Pacific Ocean and into fishing grounds.

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22
Q

What were the global impacts of the Tohoku tsunami, Japan?

A

Because Japans demand for LNG energy rose, the price of LNG increased significantly. This had the biggest impact in the Asian market, where they had the quickest rate of increasing energy consumption.

It also caused social concern surrounding nuclear power, and caused nations such as Germany to immediately shut down some of their reactors. It also caused the cost of nuclear power to rise globally, as additional safety measures had to be put in place.

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23
Q

What were the global environmental impacts of Tohoku?

A

-The radioactive debris in the water reached the coast of North America.
-Chemicals from debris of collapsing buildings were released into the atmosphere, affecting stratospheric ozone and global warming.
-One person in California was killed by Tsunami waves reached America.

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24
Q

What was the 2004 Indian Ocean Tsunami?

A

A 9.1 magnitude earthquake triggered a tsunami over 100 feet tall when it reached land. Affected many countries surrounding the ocean, such as Sri Lanka and India, and killed over 200,000 people. These deaths were from people of 46 nations, as tourists were also killed, including 543 from Sweden.

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25
Q

What were the economic impacts of the 2004 Indian Ocean tsunami?

A

-The damages were estimated at US$9.4 billion.
-600,000 lost their jobs
-Affected the supply chains of many raw materials which are exported from these SE Asian nations.

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26
Q

Do earthquakes and volcanoes cause many deaths?

A

Only 2.2% of fatalities from natural hazards are due to earthquakes, and only 0.1% are due to volcanoes.

The majority of deaths result from the slow onset hazards such as droughts and famine, rather than the rapid onset hazards.

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27
Q

What is a HILP event

A

High impact, low probability.

Tectonic mega events are often classified as this.

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28
Q

What are multiple hazard zones?

A

These are places where a number of physical hazards combine to create an increased risk for the country and its population. This is often made worse if the country’s population is vulnerable, or suffers repeated events so that there is no extended periods of time for recovery.

These places, such as the Philippines, are considered ‘disaster hotspots’.

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29
Q

What is a disaster hotspot?

A

This is a country or area that is extremely disaster prone.

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30
Q

How are hazards in multiple hazard zones linked to vulnerability over geographical space and time?

A

Being a vulnerable community makes the impacts greater, and also more challenging to manage. The magnitude of the hazard combined with the human geography of the area are important, but the hazards generally form part of a more complex web of socio-economic and environmental issues which make them harder to manage.

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31
Q

Which countries are most exposed to multiple hazards?

A

Countries in central/South America (eg Costa Rica and Chile) as well as East Asia (e.g Taiwan and the Philippines) seem to be especially vulnerable, as they are at risk of earthquakes, have coasts subject to tsunamis, may regularly experience summer cyclones as well as winter storms.

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32
Q

What % of Taiwan is exposed to multiple hazards?

A

73.1% of land in Taiwan is exposed to multiple hazard zones, and 73.1% of their population is also exposed to the 4 different hazards faced in this region.

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33
Q

Why are cities (especially mega-cities) at a high disaster risk?

A

Large urban areas are often zones of multiple, hazard risk. They tend to be centres of economic development, and can often have rapidly growing populations due to urbanisation in developing countries. This means many mega-cities have unplanned, poor quality housing in dangerous locations like river banks and steep slopes.

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34
Q

What 6 factors cause mega cities to have low hazard resilience?

A

-Concentrated political, economic and other resources.
-High population densities, particularly in old parts of cities, leads to rapid destruction and loss of life.
-Rapid growth and lack of planning causes illegal settlement of poorer people in hazardous areas.
-Ecological imbalance as rapid urbanisation destroyed ecosystems.
-High dependency on infrastructure and services in a disaster period.
-Construction of an inadequate standard.

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35
Q

What two ways can multiple hazard zones occur?

A

-when one hazard triggers the conditions necessary to make another hazard occur.
-When the hazards are completely unrelated, but occur over a short timeframe.

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36
Q

What physical vulnerabilities make the Philippines a multiple hazard zone?

A

-Violent, andesitic eruptions (e,g from Mount Mayan) are frequent. 22 active volcanoes
-Earthquakes are also frequent
-Cyclones are frequent and are usually deadly, and are linked to flooding and landslides
-Despite being rare, can have droughts from El Niño events like in 2010
-7107 islands, and is 25% bigger than the UK.

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37
Q

What human vulnerabilities make the Philippines a multiple hazard zone?

A

-High population, 109 million
-GDP of US$9200, a middle-income nation
-25% of the population lives in poverty, 2.8 million in the Capital city were squatters.
-Rapid urbanisation (urban population went from 40% in 2007 to 45% in 2010),
-Many in the rural areas lived in coastal regions, prone to flooding and storm surges.

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38
Q

What 4 major hazard events occurs in the Philippines?

A

2006 earthquake (one hazard event)
2013 Earthquake Bohol + 2013 Typhoon Haiyan (different hazards in a short space of time)

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39
Q

Causes and context of 2013 Bohol earthquake…

A

-The epicentre of the 7.1 magnitude quake was beneath the island of Bohol where two of the country’s oldest churches were damaged.
-It was the deadliest earthquake in the Philippines in 23 years since the 1990 Luzon earthquake. The energy released by the quake was equivalent to 32 of the bombs dropped in
Hiroshima.

40
Q

Impacts of the 2013 Bohol earthquake?

A

-222 were reported dead,
-8 were missing, and 976 people were injured. -more than 73,000 structures were damaged, of which more than 14,500 were totally destroyed.

Some low-rise buildings collapsed, and roads were cut in two by landslides.

41
Q

What were the impacts of the 2013 Typhoon Haiyan?

A

-Damage cost US$5.8billion
-6million lost jobs
-1.9million made homeless
-7,000 died, and sanitation issues caused a disease to break out.
-71,000 hectares of farmland were affected, and rice and corn production was destroyed.
-Oil spill caused mangrove destruction
-Many trees were uprooted

42
Q

What was the 1976 Philippine’s earthquake?

A

-9.0 magnitude earthquake
-Triggered tsunami
-Also triggered landslides, breaching the crater wall of a volcano.
-Was in the middle of the night so the population was unprepared

43
Q

What were the impacts of the 1976 Philippines earthquake?

A

-6000 died, 85% of which caused by a tsunami
-thousands injured
-Occurred in the middle of the night
-tens of thousands were made homeless

44
Q

How is the Philippines government protected against the multiple-hazards since 2009?

A

The Philippine government passed the disaster Risk Management Act to help increase resilience and reduce risk. They moved illegal settlers away from areas prone to hydro-meteorological hazards. Now has a plan for how to respond to different types of hazards and has a system to monitor volcanoes and typhoons.

45
Q

What are hydrometerological hazards?

A

The combination of the two hazards, often occur as flash flood events.

46
Q

What is prediction?

A

Prediction means knowing when or where a natural hazard will strike on a spatial and temporal scale that can be acted on meaningfully in terms of evacuation.

47
Q

What is forecasting?

A

Forecasting is much less precise than prediction, and provides a percentage chance of a hazard occurring (e.g. a 25% of a magnitude 7.0 earthquake occurring in the next 20 years). It is essentially the risk of a hazard causing a tectonic event.

48
Q

How can earthquakes be forecasted?

A

-The earthquake risk can be forecasted as it is based off of data and evidence gathered through global seismic monitoring networks as well as historical data.
-Long term forecasts (years and decades) are currently much more reliable than short-term forecasts (days).
-Forecasting is important as it encourages building regulation in areas of high stress, or can create improved evacuation procedures in areas of highest risk.

49
Q

What is one example of an earthquake being forecasted?

A

In San Fransisco, where the 1-in-100year hazard hasn’t occurred in 145 years, meaning that the risk is significant due to how overdue it is. As a result of this long-term forecast, suitable planning and preparation can occur.

50
Q

Why is it not currently possible to make accurate predictions for when and where earthquakes will occur?

A

There would need to be a ‘diagnostic precursor’, which hasn’t currently been identified. This is a characteristic pattern of seismic activity or some other physical, chemical or biological change, which would indicate a high probability of an earthquake happening in a small window of space and time.

51
Q

How are some geophysicists trying to improve their predictions of earthquakes?

A

They’re attempting to do this by calculating the underground movement of magma. They attempt to predict where the plates are running together with the most stresses, which can be a telling sign of where an earthquake may hit. They map patterns in the earths magma, and run simulations to try and locate these high stress zones.

52
Q

What do geoscientists suggest is focused on rather than improving earthquake prediction?

A

Prediction must be highly accurate to be effective, and as this isn’t a realistic prospect for the current time and foreseeable future, they suggest the main focus should instead look into improving the forecasting of earthquakes.

53
Q

What are some ways earthquakes can be monitored?

A

-Research of underground magma movement
-Animal behaviour (snakes and rats frozen to the ground)
-High levels of radon gas emissions
-Unusual electromagnetic signals.

Remember however these are all incredibly inaccurate and predicting earthquakes effectively is still a near impossible task.

54
Q

What are some ways that tsunamis can be monitored?

A

DART (Deep Ocean Assessment and Reporting Tech).
Seabed monitors recognise changes in pressure, which is then sent to surface buoys, before the data is transmitted from a satellite to ground stations where it is assessed.
This method has been used in the Pacific since 1949.

55
Q

Does tsunami monitoring accurately predict tsunamis?

A

Yes it is accurate, but the DART system can only monitor earthquakes with originate in deep water. If they occur in shallow water, e.g when an underwater landslide in Indonesia triggered a shallow tsunami close to shore, they cannot be predicted.

56
Q

How can volcanoes be monitored?

A

Volcanoes can be monitored well due to…

-Sophisticated monitoring equipment on volcanoes can measure changes as magma chambers fill and eruption nears, e.g temp rises
-Tiltmeters and strain meters record volcanoes ‘bulging’ as magma rises and seismometers record minor earthquakes indicating magma movement
-Gas spectrometers analyse gas emissions which can point to increased eruption likelihood, e.g sulphur dioxide.

57
Q

What factor can cause difficultly in volcanic eruption prediction?

A

Differences between volcanoes… Basaltic vs Andesitic/Ryholtic
-Basaltic – predicting: where the Lava will flow. Even in Hawaii the course is uncertain.
-In Heimaey, Iceland – Lava diversions in place, but in Hawaii buildings destroyed with unpredictable flows.
-Andesitic – when it will erupt. Montserrat had many false alarms at start in 1995, eventually erupted in 1997

58
Q

Why are some locations still at risk to hazards even if monitoring systems are able to make good predictions?

A

-The technology needed has to have been put in place, be functional and linked to warning systems.
-Developing nations may not be able to afford the necessary technology, e.g no warning system/monitoring tech was in place for the 2004 Indian Ocean tsunami.

59
Q

What is the hazard-management cycle?

A

This is a process in which governments and other organisations work together to protect people from the natural hazards that threaten their communities. The aim is to minimise the impacts felt by a hazard. Many key players are involved, including governments (local, national), as well as international organisations, communities and businesses.

60
Q

What are the 4 stages in the hazard-management cycle?

A

1) Mitigation: preventing hazard events or minimising their effects.
2) Preparation: preparing to deal with a hazard event
3) Response: responding effective to a hazard event to limit further damage
4) Recovery: Short term: focuses on immediate social needs of people. Long Term: get society and the economy back to normal, and reduce future vulnerability.

61
Q

What actions take place in the mitigation stage of the hazard-management cycle?

A

-Zoning and land-use planning
-Developing and enforcing building codes
-Building protective structures

62
Q

What actions take place in the preparation phase of the hazard-management cycle?

A

-Developing preparedness plans
-Developing early warning systems
-Creating evacuation routes
-Stockpiling aid equipment and supplies
-Raising public awareness

63
Q

What actions take place in the response phase of the hazard-management cycle?

A

-Search and rescue efforts
-Evacuating people where needed
-Restoring critical infrastructure (e.g power supplies)
-Ensuring critical services continue (e.g medical care and law enforcement).

64
Q

What actions take place in the recovery phase of the hazard-management cycle?

A

Short term…
-Providing essential health and safety servcies
-Restoring permanent power and water
-re-establishing transportation roots
-Providing food and temporary shelter
Long-term:
-Rebuilding homes and other infrastructure
-Re-opening businesses and schools

65
Q

What is the Park’s model?

A

The Park’s Disaster response Curve can be used to better understand the time dimensions of resilience: from a hazard striking to when a place, community or country returns to normal operations.

The x-axis shows the different stages of time, and wether relief, rehab or reconstruction has started.
The Y-axis describes quality of life, stability and infrastructure. In some cases, the quality of life can go beyond a return to normality and actually improve on where it was before the hazard event.

66
Q

What can the Park’s model be used for

A

The model can be used to help plan and understand risk and resilience, as well as to better prepare for future events, for example through modification of the responses to the event.

67
Q

What are the different stages of the disaster response curve (parks model)?

A

-Pre-disaster: QoL is normal, people do their best to prevent and prepare for the events through education and preparing supplies/medical teams
-Relief: When the event occurs. Immediate relief of emergency care and medical attention. Can last hours to days, and QoL sharply falls in this stage
-Rehabilitation: Groups (e.g government) try to return things to normal by providing food, water and shelter to those who are without basic needs.
-Reconstruction: Longer term rehab moves into the reconstruction period during which infrastructure, crops and property are invested in. This stage may also include preparation and prevention to reduce vulnerability for future events.

68
Q

How can the disaster curve on the Park’s model differ with development?

A

• Can be used to compare how areas at differing levels of development might recover.
• Impacts of the event change over time - e.g. depending on size, development, aid received
• All events have different impacts, so their curves differ - e.g. fast vs slow occurring events will have
differing responses.
• Wealthier countries will have different curves to developing as they are able to recover faster.
• For events affecting more than one area (e.g. 2004 Indian Ocean tsunami) each area will have its own
curve.

69
Q

What two factors does hazard management depend on?

A

Hazard mitigation and hazard adaptation

70
Q

What is Hazard mitigation?

A

These are strategies which are meant to avoid, delay or prevent hazard events (e.g land-use zoning, diverting lava flow, GIS mapping etc)

71
Q

What is hazard adaptation?

A

These are strategies which are designed to reduce the impacts of hazard events. (E,g high-tech monitoring, crisis mapping, modelling hazard impacts, public education and community preparedness).

72
Q

What strategies can be used to modify a tectonic event?

A

-Land-use zoning
-Hazard-resistant design
-Engineering defences
-Diversion of lava flows

73
Q

How can land-use planning be used to modify a tectonic event?.

A

Local government planners regulate how land in a community is used (e,g residential industrial etc). On areas of land, for example, vulnerable to a volcanic eruption or tsunami, land use mapping can be used to protect people and property from damage, and can choose how different land zones should be used based on how vulnerable they are.

This was used in Mount Taranaki in New Zealand.

74
Q

What are the pros and cons of land-use mapping?

A

-Allows for appropriate allocation of land based on risk
-Removes people from high risk areas and stops increased loss.
-Can prevent economic development on some high value land
-Requires good governance and strict planning rules.

75
Q

How can diverting lava flows modify a tectonic event?

A

-Lava flows can be diverted by artificial barriers which stream away from properties, and can be made from materials such as rock. 10m high barriers have been proposed in Hawaii.
-Flow can also be controlled by breaching the walls which form along the edges of flow. This was used in Mount Etna in 1983 to attempt to starve the
-In Iceland 1973, water was sprayed on lava to cool it and prevent due their spreading, which saved the port.

76
Q

What are the pros and cons of diverting lava flows to modify tectonic hazards?

A

-Can work well to give additional time to respond to a hazard and evacuate
-The terrain has to be suitable (gently downwards sloping)
-Hard to predict the path which is taken by the lava, this makes it difficult to know where to build the walls or dig the channels.
-Stopping lava from flowing towards one community may push it in the direction of another.

77
Q

What strategies can be used to modify the hazards of primary impacts from volcanoes?

A

-A house on stilts of titanium or tungsten might survive lava flow, if the stilts were strong enough to withstand the lava pushing against them.
-Airborne ash: Violent volcanoes, such as Vesuvius and Mount St Helens, tend to explode and throw up several cubic kilometres of ash and rock. A 30cm-thick ash layer can be heavy enough to cause roofs to collapse, so you’ll need a reinforced roof with a steep pitch (rather than flat) to stop the ash building up too much.
-Poisonous gas: After an eruption, pyroclastic flows can engulf a town in superheated steam and poisonous sulphur dioxide or asphyxiating carbon dioxide. To escape this, you’ll need an airtight home with an air supply – preferably underground. But ensure your access hatch doesn’t get blocked!

78
Q

How can GIS mapping be used to modify a tectonic hazard?

A

This was crucial in the Nepal 2015 earthquake, and can be used in all stages of the disaster management cycle, for example, to identify where evacuation routes should be placed, or to help with rescue and recovery options.

79
Q

What are the pros and cons of GIS mapping?

A

-Aid agencies and government can easily see where aid should be directed, as well as which communities will be the most difficult to reach.
-Tectonic hazards may not always occur as predicted, so you cannot rely on GIS mapping.
-The technology is quite advanced, and may not be available to less developed or more remote locations.

80
Q

How can hazard resistant design and engineering defences modify a tectonic event?

A

Collapsing buildings cause deaths in earthquakes. It is possible to design and construct buildings that an withstand tectonic events with planning, government monitoring and control (on building standards) in -
Developed and Developing/Emerging countries. These include steel frames, foundations, roads for easy access/evacuation. In developing nations it may include shock absorbers such as tyres, bamboo to reinforce walls, or light roofs made of plaster.

-Sea walls can also be built for tsunamis, as can mangrove forests.

81
Q

What are the pros and cons of using good building design to modify an event?

A

-Prevents death from buildings collapsing, limits falling glass, provides assembly points, easier for rescue workers and reduces rebuilding costs.
-May require good governance to enforce building codes
-Can be expensive so not available to all communities and countries.

82
Q

What strategies can be used to modify vulnerability and resilience?

A

-High tech monitoring
-Prediction
-Education
-Community preparedness and adaptation

83
Q

How can high-tech monitoring be used to modify vulnerability and resilience?

A

Technology plays an increasingly crucial role in helping communities and individuals become less vulnerable to hazard events. This includes:
-GIS to create hazard maps
-Early warning systems using scientific equipment to detect signs of a potential hazard
-Satellite communication technology helps to transmit data from monitoring equipment
-Mobile phone technology is used to communicate rapid warning systems and coordinate responses (e,g Japanese messages for the 2011 earthquake)

84
Q

What a benefits and negatives of high-tech monitoring?

A

+ Allows scientists to learn about natural processes and get better at making predictions
+Allow for advanced warning of tsunamis and volcanoes
-Public must have good access to technology for mobile warning to be effective
-Expensive and systems may require expertise to monitor

85
Q

How can crisis mapping help modify vulnerability and resilience?

A

Crisis mapping is when crowd-sourced info is used to accurately map the areas which are worst struck by a hazard, and this means the response teams can target where to help first (e,g where many people are trapped under rubble).

Was used fairly successfully following the 2010 Haiti earthquake.

86
Q

What are the pros and cons of crisis mapping?

A

+Helps rescue workers get to the worst affected more quickly
+Makes it easier for the public to share useful knowledge
-Relies on the public giving information that is factually correct and accurate

87
Q

How can education help to modify vulnerability and resilience?

A

Helps people understand what they can do to protect themselves before, during and after a hazard event, including:
- Practicing emergency procedures (Japan children practice 4 times a year) and nationwide
there is the Disaster Prevention Day is held for all.
- Encouraging households and workplaces to create emergency preparedness kits
- Education on how to construct earthquake proof buildings.

88
Q

What are the pros and cons of public education?

A

+Will help the population to be more prepared when they have to deal with the affects of a hazard
-May cause increased risk for minority groups due to inequality and marginalisation, if these poorer groups are not educated to the same degree that the rest if the population is.

89
Q

How can community preparedness and adaptation modify vulnerability and resilience?

A

Involving the actual people living in the community most at risk from a natural hazard is the best way to develop plans and educate people – especially in lower income countries. It will usually include:
-Creating a list of vulnerable people who may need special assistance
-Organising practice evaluation drills
-Providing first aid courses
-Using community knowledge (e,g 2004 Asian Tsunami, elderly in the Bay of Bengal noticed unusual movements, and saved the lives of 200 by getting them to move upland by the time the tsunami hit.

90
Q

What are the pros and cons of community preparedness and adaptation?

A

+Reduces the overall risk for the most vulnerable
+Co-ordination reduces stress when the event occurs
-May cause there to be too little focus put on the the rest of the non-high priority population.

91
Q

What strategies can be used to modify loss in a natural hazard?

A

-Role of aid
-Role of NGOs
-Role of insurers
-Role of communities

92
Q

What is the role of aid donors in modifying loss?

A

The efforts can be focused of helping communities to cope with personal, social and economic loss. Aid donors such as governments and IGOs can help by providing:
-Emergency aid (e,g providing food, clean water and shelter)
-Short-term aid (e.g restoring water supplies, providing temporary shelter)
-Long-term aid (reconstruction of buildings, infrastructure or the economy)

93
Q

What are the pros and cons of the role of aid to modify loss?

A

-money can be given straight to the gov to spend efficiently
-will support a quick return to normality and limit damages
-If the money ends up the hands of a corrupt government, it may be spent inefficiently or not spent at all (e.g Haiti gov 2010)

94
Q

What is the role of NGOs in modifying loss to a natural hazard?

A

NGOs such as OXFAM and the Red Cross play a crucial role when local governments may lack the funding or resources to respond effectively. They can provide funding, co-ordinate rescue efforts and construct reconstruction plans.
+It can often be easier to plan a response from the calm heads of a NGO rather than a panicking government
-NGOs may not know the full picture of a hazard-management cycle, and therefore the aid they provide may often be incomplete.

95
Q

What is the role of insurers on modifying loss?

A

-In 2011, the global damages from earthquakes cost US$54billion.
-Insurers can then help to limit to costs to communities, and will give individuals and businesses in developed nations the money they need to rebuild.
-In developing nations, very few people have insurance as they have other financial priorities due to being closer to absolute poverty, and those who do have very basic insurance will rarely have it cover natural hazards.

96
Q

What is the role of communities in modifying loss?

A

-As local people will always be the first to respond to a natural hazard, they will always play a crucial role in recovery. This is especially true when emergency aid may be slow, such as in Haiti when the only international airport was destroyed by the earthquake.
-However, the community may not have the necessary expertise to respond effectively, and their attempts to rescue others may be dangerous, only resulting in an increased death or injury toll.